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Temperature varies little from season to season, and Indonesia experiences relatively little change in the length of daylight hours from one season to the next; the difference between the longest day and the shortest day of the year is only forty-eight minutes. This allows crops to be grown all year round. [2]
Near these latitudes, there is one wet season and one dry season annually. At the equator there are two wet and two dry seasons, as the rain belt passes over twice a year, once moving north and once moving south. Between the tropics and the equator, locations may experience a short wet or a long wet season; and a short dry or a long dry season.
The length and severity of the dry season diminish inland (southward); at the latitude of the Amazon River—which flows eastward, just south of the equatorial line—the climate is Af. East from the Andes, between the dry, arid Caribbean and the ever-wet Amazon are the Orinoco River's Llanos or savannas, from where this climate takes its name.
The islands are in the rain shadow of Australia, and are among the driest in Indonesia. Rainfall is strongly seasonal, and April through November are generally the driest months. The windward southern side of the islands and receive annual rainfall of 2000 mm or more, with a two- to four-month dry season with less than 100 mm per month.
The Köppen climate classification is the most widely used climate classification system. [2] It defines a tropical climate as a region where the mean temperature of the coldest month is greater than or equal to 18 °C (64 °F) and does not fit into the criteria for B-group climates, classifying them as an A-group (tropical climate group). [3]
For most of Indonesia, the dry season falls between May and October while the wet season between November and April. Some regions, such as Kalimantan and Sumatra, experience only slight differences in rainfall and temperature between the seasons, whereas others, such as Nusa Tenggara, experience far more pronounced differences with droughts in ...
A dry season with a noticeable amount of rainfall followed by a rainy wet season. In essence, this version mimics the precipitation patterns more commonly found in a tropical monsoon climate, but do not receive enough precipitation during either the dry season or the year to be classified as such.
While water resources are quite abundant in Sumatra, Kalimantan, Sulawesi, Maluku and Irian, water shortages occur during the dry season in parts of Java, Bali and the Lesser Sunda Islands. In particular in Java, the dry season flows are inadequate to meet the demand, leading to irrigation shortages. [6] Irrigation accounts for 93% of water use ...